中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Zircon U-Pb and molybdenite Re-Os geochronology and whole-rock geochemistry of the Baishan porphyry Mo deposit: Insights into Triassic mineralisation and tectonic setting in the eastern Tianshan, NW China

文献类型:期刊论文

作者Wang, Yang-Shuang1; Zou, Hao2,3,4,5; Tu, Qi-Jun6; Xu, Mo1; Yang, Chang7; Fu, Yu-Zhen2
刊名GEOLOGICAL JOURNAL
出版日期2019-09-12
页码22
ISSN号0072-1050
关键词Baishan Mo deposit eastern Tianshan granite porphyry mineralisation Re-Os dating Triassic U-Pb dating
DOI10.1002/gj.3654
英文摘要The Baishan Mo deposit in the eastern Tianshan Mountains is representative of the local metallogenic Triassic Mo belt. In this study, the geological characteristics, petrography, and geochemistry of the granite porphyry and the Mo deposit were examined using zircon U-Pb dating, molybdenite Re-Os isotope dating, whole-rock geochemistry, and fluid inclusions. Results show that the crystallisation age of the Baishan granite porphyry is 229.8 +/- 1.4 Ma and the Re-Os age of molybdenite in the ore body quartz vein is 225.0 +/- 1.2 Ma. Therefore, the ore formed basically at the same time as diagenesis in the Late Triassic. The Baishan granite porphyry has high levels of Si, Al, and alkalis (K2O + Na2O = 5.72-8.88%) and low levels of Mg. The differentiation index is high (81.68-91.20), while the aluminium saturation index is low, indicating that the pluton belongs to metaluminous-weak peraluminous highly fractionated I-type granite. The rock is also enriched in light rare earth elements (LREE) and large-ion lithophile elements but depleted in heavy rare earth elements (HREE) and high-field-strength elements, with a distinct differentiation between LREEs and HREEs. delta Eu is weakly negative. The high Sr/Y and La/Yb ratios indicate geochemical characteristics similar to adakite rocks. The formation of the deposit is closely related to Mo-rich, low-salinity (1.23- to 9.73-wt.% NaCl eqv.), and medium- to low-temperature (91-280 degrees C) magmatic fluid in the plate extension setting. The magma was derived from partial melting of thickened lower crust and possibly mixed with intrusive mantle-derived magma. The ore-forming fluids were uplifted, transported, mixed with meteoric water, and precipitated to form the Mo ore.
WOS关键词I-TYPE GRANITES ; HF ISOTOPES ; AU DEPOSIT ; CONTINENTAL-CRUST ; FLUID INCLUSIONS ; SULFIDE DEPOSITS ; VERTICAL GROWTH ; EPITHERMAL AU ; YAMANSU BELT ; CU DEPOSIT
资助项目National Natural Science Foundation of China[41702108] ; National Natural Science Foundation of China[41602091] ; Sichuan Province Education Department[2018CZ0009] ; State Key Laboratory for Mineral Deposits Research[2019-LAMD-K14] ; Open Fund Project of State Key Laboratory of Lithospheric Evolution[SKL-K201902] ; China Postdoctoral Science Foundation[2019M650833]
WOS研究方向Geology
语种英语
出版者WILEY
WOS记录号WOS:000486287100001
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Sichuan Province Education Department ; Sichuan Province Education Department ; Sichuan Province Education Department ; Sichuan Province Education Department ; State Key Laboratory for Mineral Deposits Research ; State Key Laboratory for Mineral Deposits Research ; State Key Laboratory for Mineral Deposits Research ; State Key Laboratory for Mineral Deposits Research ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Sichuan Province Education Department ; Sichuan Province Education Department ; Sichuan Province Education Department ; Sichuan Province Education Department ; State Key Laboratory for Mineral Deposits Research ; State Key Laboratory for Mineral Deposits Research ; State Key Laboratory for Mineral Deposits Research ; State Key Laboratory for Mineral Deposits Research ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Sichuan Province Education Department ; Sichuan Province Education Department ; Sichuan Province Education Department ; Sichuan Province Education Department ; State Key Laboratory for Mineral Deposits Research ; State Key Laboratory for Mineral Deposits Research ; State Key Laboratory for Mineral Deposits Research ; State Key Laboratory for Mineral Deposits Research ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Sichuan Province Education Department ; Sichuan Province Education Department ; Sichuan Province Education Department ; Sichuan Province Education Department ; State Key Laboratory for Mineral Deposits Research ; State Key Laboratory for Mineral Deposits Research ; State Key Laboratory for Mineral Deposits Research ; State Key Laboratory for Mineral Deposits Research ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation
源URL[http://ir.iggcas.ac.cn/handle/132A11/93556]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Zou, Hao
作者单位1.Chengdu Univ Technol, Coll Environm & Civil Engn, State Key Lab Geohazard Prevent & Geoenvironm Pro, Chengdu, Sichuan, Peoples R China
2.Chengdu Univ Technol, Key Lab Tecton Controls Mineralizat & Hydrocarbon, Minist Land & Resources, Chengdu 610059, Sichuan, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
4.Nanjing Univ, State Key Lab Mineral Deposits Res, Nanjing, Jiangsu, Peoples R China
5.Cent S Univ, Minist Educ, Key Lab Metallogen Predict Nonferrous Met & Geol, Changsha, Hunan, Peoples R China
6.Geol Res Academe Xinjiang, Urumqi, Peoples R China
7.Chongqing Inst Geol & Mineral Resources, Inst 3, Chongqing, Peoples R China
推荐引用方式
GB/T 7714
Wang, Yang-Shuang,Zou, Hao,Tu, Qi-Jun,et al. Zircon U-Pb and molybdenite Re-Os geochronology and whole-rock geochemistry of the Baishan porphyry Mo deposit: Insights into Triassic mineralisation and tectonic setting in the eastern Tianshan, NW China[J]. GEOLOGICAL JOURNAL,2019:22.
APA Wang, Yang-Shuang,Zou, Hao,Tu, Qi-Jun,Xu, Mo,Yang, Chang,&Fu, Yu-Zhen.(2019).Zircon U-Pb and molybdenite Re-Os geochronology and whole-rock geochemistry of the Baishan porphyry Mo deposit: Insights into Triassic mineralisation and tectonic setting in the eastern Tianshan, NW China.GEOLOGICAL JOURNAL,22.
MLA Wang, Yang-Shuang,et al."Zircon U-Pb and molybdenite Re-Os geochronology and whole-rock geochemistry of the Baishan porphyry Mo deposit: Insights into Triassic mineralisation and tectonic setting in the eastern Tianshan, NW China".GEOLOGICAL JOURNAL (2019):22.

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来源:地质与地球物理研究所

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